VERTICAL PROFILE OF DENSITY IN A VAN DER WAALS ATMOSPHERE IN NATAL CITY

The van der Waals state equation for atmosphere is determined from the critical temperature and critical pressure of the air gases. The meteorological radiosonde measures atmospheric pressure, temperature, and other meteorological variables, at several altitude levels. Therefore, the diurnal and noc...

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Main Authors: Isamara de Mendonça Silva, Douglas do Nascimento Silva, Deusdedit Monteiro Medeiros
Format: Article
Language:English
Published: Instituto Federal de Educação, Ciência e Tecnologia do Rio Grande do Norte 2019-12-01
Series:Holos
Subjects:
Online Access:http://www2.ifrn.edu.br/ojs/index.php/HOLOS/article/view/8023
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author Isamara de Mendonça Silva
Douglas do Nascimento Silva
Deusdedit Monteiro Medeiros
author_facet Isamara de Mendonça Silva
Douglas do Nascimento Silva
Deusdedit Monteiro Medeiros
author_sort Isamara de Mendonça Silva
collection DOAJ
description The van der Waals state equation for atmosphere is determined from the critical temperature and critical pressure of the air gases. The meteorological radiosonde measures atmospheric pressure, temperature, and other meteorological variables, at several altitude levels. Therefore, the diurnal and nocturnal vertical profiles of the monthly average density of the atmosphere were constructed, considering the atmospheric system as an ideal gas and also as a van der Waals gas. For this purpose, the radiosonde data of the atmosphere of the metropolitan region of Natal-RN, Brazil, from 2010 to 2017, with altitude ranging from 50m to 10km.
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spelling doaj.art-4d9bb1d2cf7b4599bbf4db191da081102022-12-22T00:04:53ZengInstituto Federal de Educação, Ciência e Tecnologia do Rio Grande do NorteHolos1807-16002019-12-012011010.15628/holos.2019.80232174VERTICAL PROFILE OF DENSITY IN A VAN DER WAALS ATMOSPHERE IN NATAL CITYIsamara de Mendonça Silva0Douglas do Nascimento Silva1Deusdedit Monteiro Medeiros2Universidade Federal do Rio Grande do NorteUniversidade Federal do Rio Grande do NorteUniversidade Federal do Rio Grande do NorteThe van der Waals state equation for atmosphere is determined from the critical temperature and critical pressure of the air gases. The meteorological radiosonde measures atmospheric pressure, temperature, and other meteorological variables, at several altitude levels. Therefore, the diurnal and nocturnal vertical profiles of the monthly average density of the atmosphere were constructed, considering the atmospheric system as an ideal gas and also as a van der Waals gas. For this purpose, the radiosonde data of the atmosphere of the metropolitan region of Natal-RN, Brazil, from 2010 to 2017, with altitude ranging from 50m to 10km.http://www2.ifrn.edu.br/ojs/index.php/HOLOS/article/view/8023van der waals, atmosphere, radiosonde, vertical profile, density.
spellingShingle Isamara de Mendonça Silva
Douglas do Nascimento Silva
Deusdedit Monteiro Medeiros
VERTICAL PROFILE OF DENSITY IN A VAN DER WAALS ATMOSPHERE IN NATAL CITY
Holos
van der waals, atmosphere, radiosonde, vertical profile, density.
title VERTICAL PROFILE OF DENSITY IN A VAN DER WAALS ATMOSPHERE IN NATAL CITY
title_full VERTICAL PROFILE OF DENSITY IN A VAN DER WAALS ATMOSPHERE IN NATAL CITY
title_fullStr VERTICAL PROFILE OF DENSITY IN A VAN DER WAALS ATMOSPHERE IN NATAL CITY
title_full_unstemmed VERTICAL PROFILE OF DENSITY IN A VAN DER WAALS ATMOSPHERE IN NATAL CITY
title_short VERTICAL PROFILE OF DENSITY IN A VAN DER WAALS ATMOSPHERE IN NATAL CITY
title_sort vertical profile of density in a van der waals atmosphere in natal city
topic van der waals, atmosphere, radiosonde, vertical profile, density.
url http://www2.ifrn.edu.br/ojs/index.php/HOLOS/article/view/8023
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AT deusdeditmonteiromedeiros verticalprofileofdensityinavanderwaalsatmosphereinnatalcity